1890.] NEW-YORK MICROSCOPICAL SOCIETY. 65 



The following synonymy is made. 



1. PI. viii. fig. I. Kotalia iiiortoiii = Plano~rheliiia Utv^eriani. Thick 

 sub- variety. 



2. I'l. vii. fig. 6. Truiuatultmi Dekayi = Truitcatttliua lohatiihi: 

 Neat form. 



On page 121. — " Fulvinuliini repaitda (proper) is represented in the 

 Chalk of Masstricht, but in none of the other cretaceous beds. It is rare 

 in the Tertiaries of our Table (occurring only in the Pliocene), but is 

 scattered throughout the Atlantic. P. auricula existed in the Nummulitic 

 sea, abounded in the mid-Tertiary times, and, living now, is abundant 

 in some places ; but it is wanting in the chalk. P. Mcnaniii, however, 

 was one of the early representatives of the genus. In New Jersey 

 (North America) it occurs in the Greensand. With us it begins with the 

 white chalk, and has continued with increased prolificness till now. 

 P. Schreibersii occurs sporadically in the Greensand of New Jersey." 



On page 123, pi. ii. the Range of Recent, Tertiary, and Creta- 

 ceous RotalinK. You will notice three species as being found in the 

 Greensand of New Jersey. Plamrbulina conical, P. nautiloid, and P. 

 plano-convex. 

 1870. Herman von Credner. Die Kreide von New Jersey. 

 Zeits. d. D. Geol. Ges., xxii. 191-251. 



This article is a general review of the Cretaceous formation of New 

 Jersey, Geological and PalEeontological. On page 214 the author gives 

 under Amorphozoa a description of Flabellina cordata, Reuss, and 

 Nodosaria sulcata. Nils, of which the following is a translation. 



Flabellina cordata, Reuss. Bohm. Kr., i. 32, pi. viii. fig. 39. 

 Frondicularia ovata, Rriemer, Kr., 96, pi. xv. fig. 9. 



Elliptical, narrowly compressed, about 15 chambers with bow shaped 

 partition-walls ; the first, smallest chamber slightly nodose arched. 

 Rare in the bryozoan beds at Brownville. 

 Nodosaria sulcata. Nils. 

 Romer, Kr., 95. 



Nod. Zippei, Reuss. Bohm. Kr., i. 25, pi. viii. fig. i. 

 This handsome bodkin-shaped elongated foraminifer is on an average 

 marked by 12 deep constrictions and appears in examples 18 mm. long. 

 The small central, beak-shaped extension of the uppermost chamber and 

 its aperture for the emission of the sarcode are seldom preserved. 

 Common in the bryozoan bed at Brownville and Turtle Hill. 



N. B. — To follow : 



Part II. Original Investigations, and remarks. 



This part of the paper will consist of the determinations, 

 additions and remarks on the various species found in material 

 collected at MuUica Hill, Timber Creek, New Egypt and 

 several other localities. 



